Water Cycle and Water Security - Set 2 Flashcards
Natural causes of drought - Short term causes
- Blocking anticyclones
- Reduced soil moisture - leads to reduced evaporation
Natural causes of drought - Medium term causes
- El Nino southern oscillation (ENSO) - reduces rainfall in the western pacific
- Hydrological - reduced amounts of water in rivers or lack of precipitation which reduces amount of snow and therefore snow melt in the summer etc
Natural causes of drought - Long term causes
- Global atmospheric circulation= Descending air between Hadley and Ferrell cells creates hot and cold deserts
- Climate Change
Ecosystem functioning
- Biological, Chemical and physical processes that take place within the ecosystem
Ecosystem resilience
- Capacity of an ecosystem to recover from disturbance or withstand ongoing pressures
Wetland
Area of land saturated with water, permanently or seasonally - e.g. Everglades in Florida
Why are Wetlands important
- Act as temporary water store - mitigate river floods downstream
- Act as water filters - trap and recycle nutrients and pollutants
- Support a very diverse food web
How has drought affected wetlands
- Increased drying = more soil erosion - reduces ability to store water
- Organic soils oxidise - release carbon into the atmosphere
- Nesting sites lost etc = loss of species = gaps in the food chain
Why are rain-forests important
- 7000 drugs originate e.g. rosy periwinkle from Madagascar which treats Leukaemia
- Attracts tourists
- Prevents soil erosion
- Hardwood timber - used for construction and fuel - UK produced 13 million tonnes in 2014
Impacts of drought on forests
- takes up to 4 years for forest to recover from drought
- leads to foliage loss, More pests and diseases
- 2000 - 2003 = Severe drought led to significant die off of pinyon pines in USA - 90% died
Physical causes of desertification
- Less rainfall / drought
- Global warming
- Rivers drying up and less reliability of rainfall = vegetation dies
Human causes of Desertification
- Livestock numbers increasing = soil depleted of nutrients and land stripped of it’s protective grass cover = vegetation cannot re-establish itself
- Farmers use more land = reduced soil fertility and soil left exposed to wind and rain = vegetation removed
- Increased demand for wood = vegetation removed
Water security
Capacity of a pop to safeguard sustainable access to adequate quantities of acceptable quality of water for sustainable livelihoods and socio-economic development
Water Scarcity
Imbalance between demand and supply, classed as physical scarcity or economic scarcity - below 1000m cubed
Water stress
Country’s water consumption exceeds 10% of it’s renewable freshwater supply, including difficulties in obtaining new quantities of water - below 1700m cubed
Where is the world’s water security
- Most in Central Asia and the middle east - Least is found in Central Africa and Europe
- Anomaly’s = SE England and southern California face water insecurity
How are the worlds water supplies spread unevenly
- 60% of water supplies in 10 countries
- 66% of global pop receive only 25% of worlds annual rainfall
Water availability gap
Imbalance of water usage, with richer countries using up to 10 times more water per head
Virtual water
- AKA embedded water - embedded in all farm products, food and manufactured goods that are imported
Places likely to experience water stress
- Pakistan
- Ethiopia
- California
Places that are water vulnerable
- Spain
- Belgium
- UK
- India
Places that have sufficient water supplies - 3000m cubed per person per year
- Americas
- Russia
- Scandinavia
- Australia
Why is climate change modelling complex and uncertain
- Climate dynamics = Way the 4 systems interact with each other is only partially understood
- Global records are incomplete = hard to make future predictions
- Can be difficult to distinguish between the impacts of oscillations e.g. ENSO and Climate change
How can climate warming lead to an increase in precipitation
Increased evaporation and increase in atmospheric water holding capacity = more moisture content in the atmosphere = enhanced precipitation rates